http://lod.bco-dmo.org/id/dataset/1004723 eng; USA utf8 dataset Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project Biological and Chemical Oceanography Data Management Office (BCO-DMO) Unavailable 508-289-2009 WHOI MS#36 Woods Hole MA 02543 USA info@bco-dmo.org http://www.bco-dmo.org Monday - Friday 8:00am - 5:00pm For questions regarding this resource, please contact BCO-DMO via the email address provided. pointOfContact 2026-08-12 ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data ISO 19115-2:2009(E) Barium isotope tracer experiment results from barite–fluid laboratory equilibration experiments 2026-08-12 publication 2026-08-12 revision BCO-DMO Linked Data URI 2026-08-12 creation http://lod.bco-dmo.org/id/dataset/1004723 Tristan J. Horner Woods Hole Oceanographic Institution principalInvestigator Biological and Chemical Oceanography Data Management Office (BCO-DMO) Unavailable 508-289-2009 WHOI MS#36 Woods Hole MA 02543 USA info@bco-dmo.org http://www.bco-dmo.org Monday - Friday 8:00am - 5:00pm For questions regarding this resource, please contact BCO-DMO via the email address provided. publisher Cite this dataset as: Horner, T. J., Middleton, J. (2026) Barium isotope tracer experiment results from barite–fluid laboratory equilibration experiments. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-08-12 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/1004723 [access date] Barite–fluid barium isotope experiments Dataset Description: Methods and Sampling: &lt;p&gt;Laboratory barite–fluid equilibration experiments were conducted in the NIRVANA Labs at the Woods Hole Oceanographic Institution using trace metal clean procedures. Labware was cleaned with hydrochloric acid and nitric acid, ultra-pure reagents were used, and critical solution handling was carried out in laminar flow workbenches. Experiments used synthetic barite and artificial seawater as a marine analogue system. The barite seed material was 99.998 weight percent pure barium sulfate (Puratronic, Alfa Aesar, Lot 24177) with a nominal grain diameter of 3 micrometers. A 25 liter stock of artificial seawater with salinity 35 ± 0.5 was prepared following Smith and Chanley (1975) and adjusted to approximately pH 8.1 with concentrated potassium hydroxide. The artificial seawater stock contained a background dissolved barium concentration of 26 ± 0.8 nanomoles per liter from the reagent salts. All reactions were carried out at ambient temperature of 20 ± 2 degrees Celsius. &amp;nbsp;&lt;/p&gt; &lt;p&gt;For the isotope-tracer experiments, most dissolved barium in solution was supplied as dissolved &lt;sup&gt;135&lt;/sup&gt;Ba, whereas solid-phase barium in the seed barite possessed natural abundances. Dissolved &lt;sup&gt;135&lt;/sup&gt;Ba was derived from &lt;sup&gt;135&lt;/sup&gt;BaCO&lt;sub&gt;3&lt;/sub&gt; powder that was dissolved in hydrochloric acid and reconstituted in ultra-high purity water before addition to experiments. Experiments were carried out in duplicate in 1 liter acid-washed high-density polyethylene reactors at three initial leverage values. The amount of &lt;sup&gt;135&lt;/sup&gt;Ba spike added was adjusted based on temperature, salinity, and preexisting dissolved barium in the artificial seawater to achieve an initial barite saturation state of Ω&lt;sub&gt;barite&lt;/sub&gt; = 1.3. Reactors were agitated continuously on a New Brunswick Scientific Innova 2100 orbital shaker table. Reactors were removed from the shaker table 10 minutes before sampling to allow settling of the solid phase. Fluid aliquots of 2 milliliters were collected through time and immediately filtered through acid-cleaned 0.22 micrometer polyethersulfone membrane disc filters. A control reactor without seed barite was run under the same conditions to assess adsorption of barium to reactor walls.&lt;/p&gt; &lt;p&gt;Recovered barite samples were dissolved by alkaline conversion to barium carbonate using a modification of the method of Breit et al. (1985). Briefly, recovered solid-phase material was reacted in perfluoroalkoxy alkane vials with 1 molar sodium carbonate solution, followed by sonication, heating at 80 degrees Celsius, repeated decantation, rinsing with 18.2 megaohm-centimeter water, and final dissolution in 2 molar hydrochloric acid.&lt;/p&gt; &lt;p&gt;For isotope ratio analysis, filtered samples were diluted with 2 percent nitric acid and indium was added as an internal standard to a final concentration of 1 nanogram per milliliter. Samples were diluted and measured at salinity 1.75 to minimize non-spectral matrix effects. Filtered samples were analyzed for &lt;sup&gt;137&lt;/sup&gt;Ba:&lt;sup&gt;135&lt;/sup&gt;Ba at the Woods Hole Oceanographic Institution Plasma Facility.&lt;/p&gt; Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2023456 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2023456 onGoing Tristan J. Horner Woods Hole Oceanographic Institution 508-289-3825 266 Woods Hole Rd. Clark 448, MS# 25 Woods Hole MA 02543 United States Tristan.Horner@whoi.edu pointOfContact asNeeded Dataset Version: 1 Unknown experiment_id l_barite_initial replicate_id sample_type time_h ba137_ba135_ratio ba137_ba135_2se Thermo Fisher Scientific iCAP Q quadrupole inductively coupled plasma mass spectrometer New Brunswick Scientific Innova 2100 orbital shaker table theme None, User defined experiment id Barium replicate sample type time_elapsed featureType BCO-DMO Standard Parameters Inductively Coupled Plasma Mass Spectrometer Shaker instrument BCO-DMO Standard Instruments otherRestrictions otherRestrictions Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use. The Speed, Signature, and Significance of Barium Transformations in Seawater https://osprey.bco-dmo.org/project/885359 The Speed, Signature, and Significance of Barium Transformations in Seawater <p><em>NSF Award Abstract:</em><br /> The biological cycling of carbon in the oceans entrains many other elements, some directly (like nutrients that are essential for life) and some indirectly, as they become chemically involved in the processes that are affecting carbon. One such element is barium (Ba). Particles of the mineral barite (barium sulfate) have been found to form in association with microbial consumption of organic material in the ocean’s “twilight zone.” These particles settle to the ocean floor, and their presence in sediments has been used to infer changes in the conditions in the ocean back in time. Both the amount of barite in sediments and the isotope composition of Ba in barite are potentially sensitive to processes occurring in the twilight zone. However, several long-standing questions remain about Ba cycling in the oceans, which complicates the interpretation of barium-based proxy records. Examples of remaining questions include how much barium enters the oceans at mid-ocean ridge hydrothermal sites, and what controls the precipitation and dissolution of barite in the water column. This project seeks to tackle these questions using new approaches, on three scheduled research expeditions in the Pacific and Southern Oceans. In doing so, this project will support the education, training, and career development of a graduate student, postdoctoral researcher, and junior investigator. Undergraduate students from underrepresented groups will be recruited to conduct complementary shore-based experiments.</p> <p>This proposal seeks to answer four questions central to the utility of barium-based proxies in oceanography: What are the major inputs of new Ba to the ocean? What are their isotopic compositions? What controls the amount of pelagic barite precipitated during the remineralization of organic matter? What influences its isotopic composition? These questions will be addressed using a field-centric approach combining: in situ and shipboard tracer-incubation experiments, AUV-led adaptive sampling of Ba cycling ‘hotpots’, and section-based surveying of the surrounding oceanographic features. This multi-pronged approach will be used to investigate: the flux and isotopic composition of Ba released from the largest hydrothermal fields in the ocean, the Southern East Pacific Rise, with a focus on low-temperature venting; rates and signatures of pelagic barite precipitation associated with different phytoplankton assemblages in the Southern Ocean; and, the importance of environmental conditions, such as low ambient oxygen concentrations, in setting the efficiency of barite precipitation in the Eastern Tropical Pacific. The significance of each transformation will be assessed, which may lead to ruling out the importance of certain processes, or identifying new dependencies that could form the basis of new proxies.</p> <p>This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.</p> The Three S&#039;s largerWorkCitation project eng; USA oceans 2026-08-12 Eastern Tropical Pacific, Subtropical South Pacific, Sub-Antarctic Pacific, and Southern Oceans 0 BCO-DMO catalogue of parameters from Barium isotope tracer experiment results from barite–fluid laboratory equilibration experiments Biological and Chemical Oceanography Data Management Office (BCO-DMO) Unavailable 508-289-2009 WHOI MS#36 Woods Hole MA 02543 USA info@bco-dmo.org http://www.bco-dmo.org Monday - Friday 8:00am - 5:00pm For questions regarding this resource, please contact BCO-DMO via the email address provided. pointOfContact http://lod.bco-dmo.org/id/dataset-parameter/1004759.rdf Name: experiment_id Units: unitless Description: <p>Identifier for the experiment group in the tracer dataset</p> http://lod.bco-dmo.org/id/dataset-parameter/1004760.rdf Name: l_barite_initial Units: unitless Description: <p>Initial fraction of total barium present in the solid barite phase at the start of the experiment</p> http://lod.bco-dmo.org/id/dataset-parameter/1004761.rdf Name: replicate_id Units: unitless Description: <p>Replicate identifier for duplicate experiments</p> http://lod.bco-dmo.org/id/dataset-parameter/1004762.rdf Name: sample_type Units: unitless Description: <p>Sample type category for the row</p> http://lod.bco-dmo.org/id/dataset-parameter/1004763.rdf Name: time_h Units: hours Description: <p>Elapsed time since the start of the experiment</p> http://lod.bco-dmo.org/id/dataset-parameter/1004764.rdf Name: ba137_ba135_ratio Units: unitless Description: <p>Measured 137Ba:135Ba ratio for the sample</p> http://lod.bco-dmo.org/id/dataset-parameter/1004765.rdf Name: ba137_ba135_2se Units: unitless Description: <p>Analytical uncertainty of the measured 137Ba:135Ba ratio reported as plus or minus 2 standard error</p> GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom Biological and Chemical Oceanography Data Management Office (BCO-DMO) Unavailable 508-289-2009 WHOI MS#36 Woods Hole MA 02543 USA info@bco-dmo.org http://www.bco-dmo.org Monday - Friday 8:00am - 5:00pm For questions regarding this resource, please contact BCO-DMO via the email address provided. pointOfContact https://osprey.bco-dmo.org/dataset/1004723/data/download download onLine dataset &lt;p&gt;Laboratory barite–fluid equilibration experiments were conducted in the NIRVANA Labs at the Woods Hole Oceanographic Institution using trace metal clean procedures. Labware was cleaned with hydrochloric acid and nitric acid, ultra-pure reagents were used, and critical solution handling was carried out in laminar flow workbenches. Experiments used synthetic barite and artificial seawater as a marine analogue system. The barite seed material was 99.998 weight percent pure barium sulfate (Puratronic, Alfa Aesar, Lot 24177) with a nominal grain diameter of 3 micrometers. A 25 liter stock of artificial seawater with salinity 35 ± 0.5 was prepared following Smith and Chanley (1975) and adjusted to approximately pH 8.1 with concentrated potassium hydroxide. The artificial seawater stock contained a background dissolved barium concentration of 26 ± 0.8 nanomoles per liter from the reagent salts. All reactions were carried out at ambient temperature of 20 ± 2 degrees Celsius. &amp;nbsp;&lt;/p&gt; &lt;p&gt;For the isotope-tracer experiments, most dissolved barium in solution was supplied as dissolved &lt;sup&gt;135&lt;/sup&gt;Ba, whereas solid-phase barium in the seed barite possessed natural abundances. Dissolved &lt;sup&gt;135&lt;/sup&gt;Ba was derived from &lt;sup&gt;135&lt;/sup&gt;BaCO&lt;sub&gt;3&lt;/sub&gt; powder that was dissolved in hydrochloric acid and reconstituted in ultra-high purity water before addition to experiments. Experiments were carried out in duplicate in 1 liter acid-washed high-density polyethylene reactors at three initial leverage values. The amount of &lt;sup&gt;135&lt;/sup&gt;Ba spike added was adjusted based on temperature, salinity, and preexisting dissolved barium in the artificial seawater to achieve an initial barite saturation state of Ω&lt;sub&gt;barite&lt;/sub&gt; = 1.3. Reactors were agitated continuously on a New Brunswick Scientific Innova 2100 orbital shaker table. Reactors were removed from the shaker table 10 minutes before sampling to allow settling of the solid phase. Fluid aliquots of 2 milliliters were collected through time and immediately filtered through acid-cleaned 0.22 micrometer polyethersulfone membrane disc filters. A control reactor without seed barite was run under the same conditions to assess adsorption of barium to reactor walls.&lt;/p&gt; &lt;p&gt;Recovered barite samples were dissolved by alkaline conversion to barium carbonate using a modification of the method of Breit et al. (1985). Briefly, recovered solid-phase material was reacted in perfluoroalkoxy alkane vials with 1 molar sodium carbonate solution, followed by sonication, heating at 80 degrees Celsius, repeated decantation, rinsing with 18.2 megaohm-centimeter water, and final dissolution in 2 molar hydrochloric acid.&lt;/p&gt; &lt;p&gt;For isotope ratio analysis, filtered samples were diluted with 2 percent nitric acid and indium was added as an internal standard to a final concentration of 1 nanogram per milliliter. Samples were diluted and measured at salinity 1.75 to minimize non-spectral matrix effects. Filtered samples were analyzed for &lt;sup&gt;137&lt;/sup&gt;Ba:&lt;sup&gt;135&lt;/sup&gt;Ba at the Woods Hole Oceanographic Institution Plasma Facility.&lt;/p&gt; Specified by the Principal Investigator(s) &lt;p&gt;For isotope-tracer experiments, filtered samples were diluted with 2 percent nitric acid, indium was added as an internal standard, and &lt;sup&gt;137&lt;/sup&gt;Ba:&lt;sup&gt;135&lt;/sup&gt;Ba was measured on a quadrupole inductively coupled plasma mass spectrometer. Samples were measured at salinity 1.75 to reduce non-spectral matrix effects. Precision of the tracer ratio measurement was estimated from repeat analysis of barite samples as 4 percent relative standard deviation. The submitted tracer file reports measured &lt;sup&gt;137&lt;/sup&gt;Ba:&lt;sup&gt;135&lt;/sup&gt;Ba values and associated ±2 standard error values from the publication table.&lt;/p&gt; &lt;p&gt;The tracer file contains time-series filtered fluid samples together with recovered barite rows from the tracer experiments. Estimated dissolved barium values discussed in the paper were derived separately from blank-corrected ion beam intensities and are not the primary measurements reported in this tracer dataset. Modeled rate calculations from the reactor model are not included in this submission.&lt;/p&gt; Specified by the Principal Investigator(s) - Loaded table BCO-DMO_Tracer.xlsx,treating &quot;&quot; and &quot;nd&quot; as missing values - Renamed table bco-dmo_tracer-1 to 1004723_v1_bariumisotopes Specified by BCO-DMO Data Managers asNeeded 7.x-1.1 Biological and Chemical Oceanography Data Management Office (BCO-DMO) Unavailable 508-289-2009 WHOI MS#36 Woods Hole MA 02543 USA info@bco-dmo.org http://www.bco-dmo.org Monday - Friday 8:00am - 5:00pm For questions regarding this resource, please contact BCO-DMO via the email address provided. pointOfContact Thermo Fisher Scientific iCAP Q quadrupole inductively coupled plasma mass spectrometer Thermo Fisher Scientific iCAP Q quadrupole inductively coupled plasma mass spectrometer PI Supplied Instrument Name: Thermo Fisher Scientific iCAP Q quadrupole inductively coupled plasma mass spectrometer PI Supplied Instrument Description:Thermo Fisher Scientific iCAP Q quadrupole inductively coupled plasma mass spectrometer, Woods Hole Oceanographic Institution Plasma Facility, used for 137Ba:135Ba measurements in isotope-tracer experiments. Instrument Name: Inductively Coupled Plasma Mass Spectrometer Instrument Short Name:ICP Mass Spec Instrument Description: An ICP Mass Spec is an instrument that passes nebulized samples into an inductively-coupled gas plasma (8-10000 K) where they are atomized and ionized. Ions of specific mass-to-charge ratios are quantified in a quadrupole mass spectrometer. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB15/ New Brunswick Scientific Innova 2100 orbital shaker table New Brunswick Scientific Innova 2100 orbital shaker table PI Supplied Instrument Name: New Brunswick Scientific Innova 2100 orbital shaker table PI Supplied Instrument Description:New Brunswick Scientific Innova 2100 orbital shaker table, used for continuous agitation of experimental reactors. Instrument Name: Shaker Instrument Short Name: Instrument Description: A Shaker is a piece of lab equipment used to mix, blend, or to agitate substances in tube(s) or flask(s) by shaking them, which is mainly used in the fields of chemistry and biology. A shaker contains an oscillating board which is used to place the flasks, beakers, test tubes, etc.